| Reference Type | Journal (article/letter/editorial) |
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| Title | Radiometric Ages of Granitic Rocks, Southwestern Nova Scotia |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Cormier, R. F. | Author |
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| Smith, T. E. | Author |
| Year | 1973 (August 1) | Volume | 10 |
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| Issue | 8 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e73-106Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 473792 | Long-form Identifier | mindat:1:5:473792:0 |
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| GUID | 0 |
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| Full Reference | Cormier, R. F., Smith, T. E. (1973) Radiometric Ages of Granitic Rocks, Southwestern Nova Scotia. Canadian Journal of Earth Sciences, 10 (8) 1201-1210 doi:10.1139/e73-106 |
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| Plain Text | Cormier, R. F., Smith, T. E. (1973) Radiometric Ages of Granitic Rocks, Southwestern Nova Scotia. Canadian Journal of Earth Sciences, 10 (8) 1201-1210 doi:10.1139/e73-106 |
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| In | (1973, August) Canadian Journal of Earth Sciences Vol. 10 (8) Canadian Science Publishing |
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| Abstract/Notes | Granitic rocks comprising the eastern half of the main batholith of southwestern Nova Scotia have been studied. The granitic rocks intrude Lower Paleozoic metasediments of the Meguma Group. Field work, the chemistry and petrology of the granitic rocks, and Rb–Sr whole-rock isochron dates indicate that there were at least two episodes of granite emplacement, the earlier about 415 m.y. ago and the later about 350 m.y. ago. Samples from a much smaller pluton some 65 mi (104 km) away from the study area were also dated and are correlated with rocks in the main batholith. |
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